Go to content

finlo.cottier@sams.ac.uk
UiT Norges arktiske universitet

Year: 2019
Project manager: Finlo Cottier
Project code: 582018

It is apparent that across the Arctic, the cryosphere is changing at an accelerated speed. One manifestation is the increasing rate at which glaciers are releasing freshwater, nutrients and suspended material into the marine system. The circulation within fjords is highly modified by glacial runoff and our ability to model fjord dynamics is dependent on appropriate representation of the freshwater fluxes from the glacier. Further, the influence that areas of high freshwater content have on fjordic ecosystems is the subject of current debate. Ecological dynamics at glacier fronts are poorly studied and the input of subsurface plumes of freshwater discharged from the glacier has been hypothesized to kill or immobilize zooplankton through an osmotic shock. This, in turn, is proposed to impact functioning of higher trophic levels. This proposal looks at the physical and ecological impacts of increased input of freshwater from melting glaciers. We recognize that there is a fundamental lack of empirical data obtained from these challenging habitats, yet a clear understanding of the oceanographic and ecological gradients at the ocean-glacier margin is crucial to understand climate change effects in terms of ocean exchange processes, carbon transport and ecosystem services and food web interactions. Significantly, these regions are very difficult to access and to obtain spatially relevant data in order to map and chracterise the extreme gradients.

Frost proof websites from: Gnist